(1988) Pleistocene-holocene sedimentation along King fahd Causeway between Saudi Arabia and Bahrain. Masters thesis, King Fahd University of Petroleum and Minerals.
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Arabic Abstract
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English Abstract
This study was conducted on a series of 10 rock cores, as much as 44 meter long, along King Fahd causeway between Saudi Arabia and Bahrain at the entrance of Gulf of Salwa (26 N-50 20 E) on the Arabian Shallow shelf. The cores penetrate Pleistocene-Holocoene rocks and sediments in that area of the Arabian Gulf. These cores show two mineralogical units. 1- A lower dolomite interval, as much as 40 meters thick. 2- An upper non-dolomite interval, three to nine meters thick, which consists of interbedded quartz sandstone, calcitic skeletal grainstone, quartz sand, aragonitic skeletal and oolitic sand and grainstone. The dolomitic interval comprises several depositional cycles. Each cycle includes upward shallowing sequence consisting of
| Item Type: | Thesis (Masters) |
|---|---|
| Subjects: | Earth Sciences |
| Department: | College of Petroleum Engineering and Geosciences > Geosciences |
| Committee Advisor: | Conley, Curtis D. |
| Committee Members: | Lynts, G. W. and Cagatay, Mehmet Namik |
| Depositing User: | Mr. Admin Admin |
| Date Deposited: | 22 Jun 2008 13:50 |
| Last Modified: | 01 Nov 2019 13:51 |
| URI: | http://eprints.kfupm.edu.sa/id/eprint/9836 |